Weather Alert in Indiana
Flood Warning issued March 4 at 5:55AM EST until March 4 at 7:15PM EST by NWS Indianapolis IN
AREAS AFFECTED: Owen, IN
DESCRIPTION: ...The National Weather Service in Indianapolis IN has issued a Flood Warning for the following rivers in Indiana... Mill Creek near Cataract. .Between 2 and 4 inches of rain have fallen across central Indiana as of early Wednesday morning. Up to 2 inches have fallen in south-central Indiana. This has led creeks to rise above flood stage and rivers will follow in the coming days. Additional rain is in the forecast over the next several days. * WHAT...Minor flooding is forecast. * WHERE...Mill Creek near Cataract. * WHEN...From early this morning to this evening. * IMPACTS...At 15.0 feet, Mill Creek at flood stage. Camp Otto Road begins to flood. Low pasture land along Mill Creek begins to flood. * ADDITIONAL DETAILS... - At 5:15 AM EST Wednesday the stage was 14.9 feet. - Forecast...The river is expected to rise to a crest of 15.4 feet late this morning. It will then fall below flood stage this afternoon. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/ind. The next statement should be issued this evening by around 715 PM EST.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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